Ra. Irving, NEAR-SHORE BATHYMETRY AND REEF BIOTOPES OF HENDERSON ISLAND, PITCAIRNGROUP, Biological Journal of the Linnean Society, 56(1-2), 1995, pp. 309-324
The coral reef which surrounds two thirds of Henderson Island, Pitcair
n Group, consists of a reef aat, reef margin and fore-reef which slope
s gradually into deeper water. The range of sublittoral habitats provi
ded by this topography is limited, reflecting a low level of coral div
ersity. Spur and groove formations of the fore-reef are present around
the northern end of the island which contrasts with the south-western
corner, where, in the absence of a hinging reef platform, subaerial c
liff faces are fronted by a cliff foot submarine 'trench'. In general,
live coral cover on the fore-reef was estimated at between 10-30%, th
ough at sites off the east coast it reached 80%. The associated commun
ities, particularly of sessile filter-feeding groups, were found to be
impoverished. The two factors of biogeographical isolation and of loc
al bioerosion processes are proposed as being the main reasons for the
depauperate nature of the island's reef. Brief notes are included on
the lagoon and fore-reef bathymetry and habitats of Ducie and Oeno Ato
lls for comparative purposes. (C) 1995 The Linnean Society of London